Distribution, diversity, and habitat partitioning of ...

Anais da Academia Brasileira de Ciências (2019) 91(1): e20170973 (Annals of the Brazilian Academy of Sciences)Printed version ISSN 0001-3765 / Online version ISSN 1678-2690http://dx.doi.org/10.1590/0001-3765201920170973www.scielo.br/aabc | www.fb.com/aabcjournal

An Acad Bras Cienc (2019) 91(1)BIOlOgICAl SCIeNCeS

Distribution, diversity, and habitat partitioning of Scolecitrichidae species (Copepoda: Calanoida) down to 1,200 m in the Southwestern Atlantic Ocean

CRISTINA O. DIAS1, ADRIANA V. DE ARAUJO2 and SÉRGIO L.C. BONECKER1

1laboratório Integrado de Zooplâncton e Ictioplâncton, Departamento de Zoologia, Instituto de Biologia, Centro de Ciências da Saúde, Universidade Federal do Rio de Janeiro, Avenida Prof. Rodolpho

Rocco, 211, Bl. A, Sala A0-084, Ilha do Fundão, 21941-590 Rio de Janeiro, RJ, Brazil2Instituto Federal de educação, Ciência e Tecnologia do Rio de Janeiro, Campus

Resende, Rua Prefeito Botafogo, s/n, 27541-030 Resende, RJ, Brazil

Manuscript received on November 28, 2017; accepted for publication on July 13, 2018

How to cite: DIAS CO, ARAUJO AV AND BONeCKeR SlC. 2019. Distribution, diversity, and habitat partitioning of Scolecitrichidae species (Copepoda: Calanoida) down to 1,200 m in the Southwestern Atlantic Ocean. An Acad Bras Cienc 91: e20170973. DOI 10.1590/0001-3765201920170973.

Abstract: In this study, we analyzed the main distributional features of Scolecitrichidae species in the Southwestern Atlantic Ocean (northern region of Rio de Janeiro State) and determined and described their habitat partitioning, based on a night series of stratified samplings down to a depth of 1,200 m. A total of 18 species from seven genera were identified and grouped according to their depth distribution. Distinct vertical patterns of total density, richness, diversity, and evenness were observed, with a decrease in density and an increase in diversity and richness with increasing depth. The total scolecitrichid abundance was dominated by a few epipelagic migrant species (Scolecithrix danae, Scolecithricella minor, Amallothrix tenuiserrata, and Lophothrix frontalis). The nondominant species were distributed in different habitats in the mesopelagic layer (upper-mesopelagic, mesopelagic, and lower-mesopelagic species) according to their vertical patterns of abundance and occurrence in the two sampling periods (rainy and dry season). The total density of scolecitrichid copepods was positively related to temperature and nitrate, and negatively related to silicate at 1 m depth. The abundance of scolecitrichids copepods in the upper layer with warm and oligotrophic waters supports the hypothesis of the influence of different water masses on the scolecitrichid assemblage. High abundance of appendicularians (Oikopleura longicauda) at 1 m depth in the region implies a high production rate of discarded “houses”, an important dietary component for Scolecitrichidae copepods. The observed patterns of seasonal cycles and vertical distribution suggest that the diverse scolecitrichid assemblage in the region may be structured mainly according to the partitioning of vertical habitats and food resources.Key words: Copepoda, Scolecitrichid, deep waters, Southwestern Atlantic Ocean, Tropical environment.

Correspondence to: Cristina de Oliveira Dias e-mail: [email protected] ORCid: http://orcid.org/0000-0001-8359-0234

INTRODUCTION

The Scolecitrichidae (Copepoda: Calanoida) are

widely distributed throughout the world’s oceans, with peak abundance in the tropics (gopalakrishnan and Devi 1998, el-Sherbiny and Al-Aidaroos 2013). Scolecitrichidae are one of the most species-rich families of calanoid copepods (Boxshall

CRISTINA O. DIAS, ADRIANA V. De ARAUJO and SÉRgIO l.C. BONeCKeR SCOleCITRICHIDAe SPeCIeS OF THe SOUTHWeSTeRN ATlANTIC

An Acad Bras Cienc (2019) 91(1) e20170973 2 | 17

and Halsey 2004, Kuriyama and Nishida 2006), and have generally been found from pelagic to benthopelagic regions in marine waters below 200 m (Ferrari and Markhaseva 2000, Markhaseva and Dahms 2004, el-Sherbiny and Al-Aidaroos 2013).

like several families distributed primarily in the meso-, bathy-, and benthopelagic layers, scolecitrichids are consumers of detritus particles and play important roles in the oceanic food web, contributing to the remineralization of organic particles and transferring small organic particles to higher trophic levels (Steinberg 1995, Nishida and Ohtsuka 1997). Kuriyama and Nishida (2006) have suggested that the scolecitrichids provide an excellent model group of zooplankton for understanding the structural aspects of species diversity and of niche-partitioning in the oceanic environment, in relation to their patterns of vertical distribution, feeding specialization, and taxonomic relationships.

Currently, 32 genera are included in the family Scolecitrichidae (Razouls et al. 2005-2018), 20 of which were first described in the 21st century (Ferrari and Markhaseva 2000, el-Sherbiny and Al-Aidaroos 2013), which reflects a general rise in interest in the biology of deep ocean waters in recent years (Ferrari and Markhaseva 2000). The vertical distribution of scolecitrichids has been studied in the Atlantic, Pacific, Indian, and Antarctic oceans, however these studies have dealt with calanoid copepods as a whole (Madhupratap and Haridas 1986, Yamaguchi et al. 1999, Wishner et al. 2008) and have generally analyzed only a limited number of scolecitrichid species and/or specimens (Vyshkvartzeva 2001, Ohtsuka et al. 2002, el-Sherbiny and Al-Aidaroos 2013). even though substantial information on the taxonomy of scolecitrichid copepods is available, their vertical distribution patterns and phylogenetic taxonomic relationships (i.e., within genera) are still poorly known (Kuriyama and Nishida 2006). Moreover, there have been no comprehensive studies of

scolecitrichid zoogeography in the Southwestern Atlantic Ocean.

In the Southwestern Atlantic Ocean, most studies have investigated zooplankton distribution only in the epipelagic zone in neritic and oceanic regions (Berasategui et al. 2006, eskinazi-Sant’anna and Björnberg 2006, lopes et al. 2006, Dias et al. 2010, 2015, 2018, Bonecker et al. 2014, 2018), and knowledge of Scolecitrichidae distribution ranges is restricted to a few epipelagic species. Thus, information on mesopelagic and bathypelagic Scolecitrichidae in the SW Atlantic Ocean is limited (Campaner 1984, Dias et al. 2010, 2018, Bonecker et al. 2014, 2018), and their vertical distribution patterns and phylogenetic relationships have not yet been thoroughly described.

The Campos Basin is located on the SW boundary of the South Atlantic Ocean, and its copepod community has previously been investigated (Campaner 1984, Dias et al. 2010, 2015, 2018, Bonecker et al. 2014, 2018), with high (ca. 20) scolecitrichid species richness reported. The aim of this study was to investigate the abundance patterns and vertical distribution of scolecitrichid copepods in the northern region of Rio de Janeiro State in order to better understand the species diversity and habitat partitioning of this family in the deep sea (down to a depth of 1,200 m). We discuss possible mechanisms for species segregation and aspects of their temporal and geographic variability. We ascertain the potential relationships between Scolecitrichidae distribution patterns and environmental variables and contribute to elucidating the vertical distribution of this family in a tropical oceanic region.

MATERIALS AND METHODS

HYDROgRAPHY OF THe STUDY AReA

The Campos Basin occupies a portion of the Brazilian continental boundary between southern espírito Santo (Vitória High, 20.5°S) and northern



SAMPleS COlleCTION AND ANAlYSeS

Mesozooplankton (> 200 μm) samples were collected during oceanographic cruises from February 25 to April 13, 2009 (rainy season, RS) and from August 5 to September 17, 2009 (dry season, DS). The sampling stations were distributed along six transects perpendicular to the coast (A, C, D, F, H, and I) in a north–south direction. each transect contained eight sampling stations (four on the continental shelf and four on the slope) between the 25-m and 3,000-m isobaths (25, 50, 75, 150, 400, 1,000, 1,900, and 3,000 m; Figure 2). Zooplankton samples were not collected in transects B, e, and g. All samples were collected between 6:18 pm and 5:08 am during the RS and between 5:57 pm and 5:46 am during the DS (local time).

environmental data recorded included the following: (a) water temperature and salinity at all sampling depths, namely, 1 m, 250 m, 800 m, and 1,200 m, by using a CTD sonde; (b) inorganic nutrients (nitrate, silicate, and orthophosphate), determined by standard oceanographic methods (Grasshoff et al. 1999); (c) DO, measured continuously in the water column using a sensor coupled to the CTD; and (d) suspended particulate matter (SPM), obtained from 4-l water subsamples filtered through a Whatman GF/F filter pre-combusted at 510°C for 4 h, and weighed to an accuracy of 0.0001 g. Detailed methodology and discussion of the hydrochemistry of the study area are presented elsewhere (Bonecker et al. 2014, Rodrigues et al. 2014, Dias et al. 2015, Suzuki et al. 2015).

Mesozooplankton samples were collected by horizontal hauls at the same stations and depths (1 m, 250 m, 800 m, and 1,200 m) at which the environmental parameters were recorded. Sampling depths represent the nucleus of each water mass. In the DS, no samples were collected on the 3,000-m isobaths of transects H and I, due to logistical problems. A total of 193 samples (102 in the RS and 91 in the DS) were collected using a Hydro-

Rio de Janeiro (Cabo Frio High, 24°S), covering an area of approximately 100,000 km2 (Viana et al. 1998). This region is characterized by its water column structure and water mass distribution over the continental shelf and slope. The different water masses in the area have distinct temperatures, salinities, and dissolved oxygen (DO) levels that provide different habitats for pelagic species down to depths of 3,000 m.

The Brazil Current (BC) is a warm, oligotrophic western boundary current that flows southwest, as part of the South Atlantic western boundary current system (Stramma et al. 1990). The upper reaches of the water column include the nutrient-poor Tropical Water [TW; temperature (T) > 20°C; salinity (S) > 36.20] and the relatively cold, nutrient-rich South Atlantic Central Water (SACW, 142–567 m depth; 8.72°C < T < 20°C and 34.66 < S < 36.20) that flows along the continental slope at the bottom layer of the BC (Bonecker et al. 2014, Dias et al. 2015). Water masses at greater depths include the cold Antarctic Intermediate Water (AAIW, 567–1,060 m; 3.46°C < T < 8.72°C and 34.42 < S < 34.66), which flows north, has high values of phosphate, is rich in oxygen, and is less saline (Viana et al. 1998, Pedrosa et al. 2006), and the Upper Circumpolar Water (UCDW, 1,060–1,300 m; 3.31°C < T < 3.46°C and 34.42 < S < 34.66) that can be identified only by chemical analysis due to its lower levels of oxygen and higher concentration of nutrients, mainly silicates (Pedrosa et al. 2006). Finally, the North Atlantic Deep Water (NADW; 2.04°C < T < 3.31°C and 34.59 < S < 34.87) is found below the UCDW, influencing the lower continental slope below a depth of 1,300 m (Mémery et al. 2000, Silveira et al. 2000; Figure 1). This southward-flowing water mass is highly saline, oxygen-rich, and nutrient-poor compared with the Circumpolar Water (upper and lower) (Viana et al. 1998, Pedrosa et al. 2006).



Bios MultiNet® type midi with a 50 × 50 cm frame opening (aperture of 0.25 m2) and dimensions of 80 cm × 90 cm × 95 cm. The MultiNet was equipped with a set of nets (mesh apertures of 200 µm) and a different net was used to sample each water mass to prevent contamination. At each predetermined depth, hauls were performed at a speed of 2 knots using an opening–closing mechanism operated by electronically transmitted commands. The depth of the haul was controlled during the entire procedure to ensure that the net was towed horizontally. At 1 m depth, 5-minute hauls were performed, whereas at 250 m, 800 m, and 1,200 m depths, the net was

towed for 10 minutes because of the lower density of organisms in deeper waters. To determine the collecting depth, the MultiNet was equipped with a depth sensor. A depressor was used to maintain net stability. Water volume and haul depth data were transmitted in real-time to a shipboard computer. Filtration efficiency and water volume were determined using two flow meters: one was mounted in front of the mouth of the net and the other fixed to the outer part of the net. Filtered water volume in each sampling depth ranged from 60 to 280 m3 (1 m), from 57 to 195 m3 (250 m), from 83 to 269 m3 (800 m), and from 92 to 264 m3 (1,200 m).

Samples were immediately fixed and preserved in 4% buffered formalin. In the laboratory, the preserved samples were divided into between 1 and 10 fractions using a Folsom Plankton Splitter (Hydro-Bios, Am Jägersberg, Altenholz, germany) (Mcewen et al. 1957) and the resultant subsamples were analyzed. The degree of subsampling was adjusted to the density of the organisms so that at least 100 individuals were sorted in each sample. All the copepods were sorted, identified (adults and copepodites), and counted under a stereoscopic microscope, and the scolecitrichid copepods were identified according to the methods of Bradford-grieve et al. (1999) and Dias and Araujo (2006). Taxon abundance per cubic meter and scolecitrichid species composition were determined for all samples. All collected specimens were deposited in the copepod collection of the Integrated Zooplankton and Ichthyoplankton laboratory of the Universidade Federal do Rio de Janeiro.

DATA ANAlYSIS

The scolecitrichids were classified according to their vertical distribution in the studied area based on criteria developed by Kuriyama and Nishida (2006), which classified the scolecitrichid species into six groups (epipelagic migrants, interzonal

Figure 1 - Salinity and temperature of the five water masses (0-3,260 m) in the Campos Basin, central Brazilian coast, modified from Bonecker et al. (2014). Solid line, temperature; dashed line, salinity; TW, Tropical Water; SACW, South Atlantic Central Water; AAIW, Antarctic Intermediate Water; UCDW, Upper Circumpolar Deep Water; NADW, North Atlantic Deep Water.



migrants, upper-mesopelagic migrants, upper-mesopelagic non-migrants, lower-mesopelagic species, and mesopelagic species) according to their distributional depths and day–night differences. These criteria were modified for adaptation to local conditions.

For comparisons of diversity between the sampling periods and depths, the Shannon–Wiener index (H′) was calculated for each station as follows:

H′ = −∑pi ∗ ln (pi),

where pi is the fraction of species i in the total sample. We also calculated Pielou’s index of evenness. These analyses were run using the PRIMeR 6.0 package (Clarke and gorley 2006). The vertical (depth) and temporal (RS and DS) differences in density, richness, diversity, and evenness of scolecitrichids, and their interactions

were analyzed using generalized linear models (GLMs) with gamma family (dispersion = 1). A low additive constant (1) was applied to the density data from each sampling station data to eliminate zero values in the matrix because the gamma family does not allow for zeros. The results were considered significant at a significance level < 0.05. The analyses were performed using R 3.1.3 (R Core Team 2015; www.r-project.org).

The influence of environmental parameters on Scolecitrichidae family distribution was analyzed using glMs with gamma family. The descriptor was the total scolecitrichid density, whereas the environmental parameters were used as predictor variables to describe the total scolecitrichid density. Initially, a full model was designed using all the variables, and then biologically logical models were constructed containing fewer variables. To

Figure 2 - Study area showing the sampling stations and collection sites (black solid circles) for specimens of scolecitrichids used in this study.



minimize collinearity effects on the results, highly correlated variables (salinity and orthophosphate) were excluded from the analysis. The environmental parameters used were temperature, SPM, dissolved oxygen (DO), nitrate (NO3), and silicate. From the results of this full model, biologically important models were designed containing fewer predictor variables. The Akaike information criterion for small samples (AICc) was used to select the best model among those constructed. The model with the lowest AICc was considered the most plausible for describing the data, and the importance of alternative models was estimated from the difference between AIC values (ΔAICc). Models with ΔAICc ≤ 2 were also considered plausible (Burnham and Anderson 2002). The analyses were performed using R 3.1.3 (R Core Team 2015; www.r-project.org) and the MuMIn package.

RESULTS

HYDROgRAPHY

environmental conditions during the study period have been described in detail by Bonecker et al. (2014), Rodrigues et al. (2014), Dias et al. (2015), and Suzuki et al. (2015), and are therefore only briefly summarized here and in Table I.

At 1 m depth, the lowest values of temperature and salinity were recorded during the DS, mainly at stations located in the southern part of the study area, over the continental shelf near Cabo Frio, and in the northern part, under the continental influence of the Paraíba do Sul River. During the RS, the lowest values were only recorded near Cabo Frio. At 250 m, the highest temperature values were measured under the continental influence of the Paraíba do Sul River (RS) and over the continental shelf near Cabo Frio (DS). At 800 m and 1,200 m, both temperature and salinity were relatively uniform. During the two sampling periods, the values of SPM declined above the slope compared with the continental shelf, and along the water column with increasing depth. The

TAB

LE

IM

inim

um a

nd m

axim

um v

alue

s reg

iste

red

for

the

para

met

ers t

empe

ratu

re (°

C),

salin

ity, s

uspe

nded

par

ticul

ate

mat

ter

(SPM

, mg

L-1),

diss

olve

d ox

ygen

(DO

), ni

trat

e (μ

mol

L-1),

silic

ate

(μm

ol L

-1),

and

orth

opho

spha

te (μ

mol

L-1) f

or sa

mpl

es c

olle

cted

in th

e w

ater

col

umn

of th

e C

ampo

s Bas

in d

urin

g th

e ra

iny

(RS)

and

dry

(D

S) se

ason

s of 2

009.

Dep

htSa

mpl

ing

Peri

ods

Tem

pera

ture

(°

C)

Salin

itySP

M (m

g L

-1)

DO

(mg

L-1)

Nitr

ate

(μm

ol

L-1)

Silic

ate

(μm

ol

L-1)

Ort

hoph

osfa

te

(μm

ol L

-1)

Min

Max

Min

Max

Min

Max

Min

Max

Min

Max

Min

Max

Min

Max

1 m

Rai

ny S

easo

n24

.82

28.5

035

.44

37.2

80.

293.

995.

786.

530.

563.

090.

419.

060.

010.

14

Dry

Sea

son

19.6

424

.89

35.7

137

.12

0.15

6.50

4.36

7.75

0.37

4.85

0.31

7.89

0.02

0.44

250

m

Rai

ny S

easo

n13

.64

25.6

535

.28

35.9

90.

041.

936.

176.

680.

587.

670.

583.

530.

020.

71

Dry

Sea

son

12.0

916

.75

35.1

235

.79

0.17

0.87

6.22

6.77

1.48

11.4

11.

357.

150.

260.

81

800

m

Rai

ny S

easo

n4.

645.

6134

.33

34.4

00.

011.

026.

036.

845.

2932

.37

5.33

30.1

50.

722.

00

Dry

Sea

son

4.39

5.33

34.3

434

.46

0.22

0.67

6.08

6.67

18.1

834

.72

19.8

531

.31

1.69

1.95

1,20

0 m

Rai

ny S

easo

n3.

203.

5334

.45

34.5

70.

331.

115.

906.

0617

.58

31.7

620

.93

51.1

11.

712.

08

Dry

Sea

son

3.19

3.45

34.5

434

.67

0.13

1.05

5.76

5.89

25.4

235

.33

37.5

449

.88

1.79

2.07



minor, Amallothrix tenuiserrata, and Lophothrix frontalis were the most frequent (≥ 5% of the total stations) and abundant (97% of the total Scolecitrichidae collected; Table II). The remaining 14 species were less abundant and frequent (Table II). During the sampling period, some species showed seasonal changes: Scaphocalanus brevicornis , Scaphocalanus magnus , and Scolecithrix bradyi occurred only during the RS, whereas Scaphocalanus elongatus, Lophothrix latipes, Racovitzanus levis, Scaphocalanus subbrevicornis, Pseudoamallothrix ovata, Pseudoamallothrix profunda, and A. tenuiserrata occurred only during the DS (Table II).

As for the total scolecitrichid density, the species richness did not vary between the sampling periods, although it did vary among the sample depths (p < 0.05). There were interactions between the effects of the sampling periods and depths on the diversity and evenness of scolecitrichids (p < 0.05). During the RS, the species richness ranged from 1 to 3, with the diversity (H′) varying from 0.00 to 1.58, whereas during the DS, the number of species varied from 1 to 4 species, and the diversity ranged from 0.00 to 2.00. In both sampling periods, the evenness ranged from 0.00 to 1.00. The number, diversity, and evenness of species showed gradual increases with depth, with an increasing trend during the DS at 800 and 1,200 m (Figure 3b). In terms of species numbers, Scaphocalanus was the most species-rich genus (five species observed during the sampling periods), followed by Lophothrix (three species). Scaphocalanus was represented by three species in each sampling period, whereas the species richness of Lophothrix increased during the DS (RS: two species, DS: three species; Table II).

In the RS, the single species that occurred at 1 m depth, above both the continental shelf and slope, was S. danae (continental shelf: 4.56 ± 11.98 ind.m-3; slope: 4.54 ± 15.52 ind.m-3). In waters above the continental shelf, this species was found at stations located in the southern (in the 150-m

highest values of SPM were recorded in the southern part of the study area (Cabo Frio region) during the DS. Dissolved Oxygen values were relatively homogeneous in both sampling seasons, except for those at 1 m depth, where both low and high values were obtained during the DS over the continental shelf of the northern part of the study area (under the continental influence of the Paraíba do Sul River). In both sampling periods, a nutrient pattern typical of that in oceans was observed, characterized by low values at the surface and increasing with depth. At 1 m depth, the highest values were observed over the continental shelf during the DS, particularly in the Cabo Frio region.

ABUNDANCe, OCCURReNCe, AND VeRTICAl DISTRIBUTION OF SCOleCITRICHID COPePODS

Scolecitrichidae species comprised ca. 1% of total copepod abundance, although this family was the most species-rich in the study area (13% of total copepod taxa; Bonecker et al. 2015). Although the total scolecitrichid abundance did not vary between the sampling periods, it did show variation among sample depths (p < 0.05). The abundance of scolecitrichids showed a distinct pattern, with the major population occurring at 1 m (mean values—RS: 6.94 ± 16.76 ind.m-3; DS: 28.07 ± 88.00 ind.m-3) and at 250 m (mean values—RS: 2.45 ± 2.99 ind.m-3; DS: 4.85 ± 14.24 ind.m-3), decreasing with depth in the two sampling periods (Figure 3a). The highest scolecitrichid abundances were recorded over the continental shelf (mean values—RS: 7.50 ± 17.48 ind.m-3; DS: 32.93 ± 115.08 ind.m-3) in comparison with the slope (mean values—RS: 2.82 ± 9.45 ind.m-3; DS: 9.28 ± 28.40 ind.m-3). The highest densities found above the continental shelf were recorded near Cabo Frio and under the influence of the Paraíba do Sul River during the DS.

Twenty-four copepod taxa were identified, including 18 species of Scolecitrichidae belonging to eight genera. Scolecithrix danae, Scolecithricella



TABLE IIMean, standard deviation (ind.·m-3), and occurrence frequency (%) of scolecitrichid species at different depths in Campos

Basin during the two sampling periods.

Species/StationsRainy season

1 m 250 m 800 m 1,200 mAmallothrix dentipes - - - 0.01±0.04/8.33

Amallothrix tenuiserrata - - - -Lophothrix frontalis - 0.03±0.10/8.33 0.01±0.02/11.11 0.01±0.02/16.67Lophothrix latipes - - - -

Lophothrix quadrispinosa - 0.01±0.04/4.17 - -Pseudoamallothrix ovata - - - -

Pseudoamallothrix profunda - - - -Racovitzanus levis - - - -

Scaphocalanus brevicornis - - 0.002±0.01/5.56 -Scaphocalanus echinatus - 0.25±1.25/4.17 0.004±0.01/11.11 -Scaphocalanus elongatus - - -Scaphocalanus magnus - - 0.004±0.02/5.56 0.01±0.03/16.67

Scaphocalanus subbrevicornis - - -Scolecithrix danae 4.55±13.71/ 16.67 0.31±1.37/12.50 0.08±0.31/16.67 0.05±0.10/41.67Scolecithrix bradyi - 0.01±0.03/4.17 - 0.001±0.002/8.33

Scolecithricella dentata - 0.20±0.81/12.50 0.01±0.02/5.56 -Scolecithricella minor - 1.27±2.71/29.17 0.04±0.13/16.67 -

Scottocalanus securifrons - 0.03±0.09/12.50 - -

Species/StationsDry season

1 m 250 m 800 m 1,200 mAmallothrix dentipes - - 0.002±0.01/6.67 0.005±0.01/12.50

Amallothrix tenuiserrata 0.85±2.99/13.04 1.35±5.71/27.27 - 0.01±0.04/12.50Lophothrix frontalis 0.13±0.87/2.17 0.01±0.06/4.55 - 0.002±0.004/25.00Lophothrix latipes - - 0.10±0.38/6.67 -

Lophothrix quadrispinosa - - - 0.004±0.01/12.50Pseudoamallothrix ovata - 0.03±0.12/9.09 - -

Pseudoamallothrix profunda - 0.001±0.01/4.55 - -Racovitzanus levis - 0.01±0.05/4.55 - -

Scaphocalanus brevicornis - - - -Scaphocalanus echinatus - 0.04±0.09/18.18 - -Scaphocalanus elongatus - - - 0.001±0.02/12.50Scaphocalanus magnus - - - -

Scaphocalanus subbrevicornis - - - 0.001±0.002/12.50Scolecithrix danae 0.33±1.19/8.70 0.02±0.07/9.09 - -Scolecithrix bradyi - - - -

Scolecithricella dentata - 0.05±0.13/13.64 - 0.003±0.01/25.00Scolecithricella minor 2.73±12.59/6.52 2.67±8.65/36.36 0.12±0.42/13.33 0.01±0.04/25.00

Scottocalanus securifrons - 0.001±0.01/4.55 0.10±0.38/6.67 -



isobath) and northern (in the 50-m and 75-m isobaths) parts of the study area (Figure 4a). During the DS, L. frontalis (0.24 ± 1.20 ind.m-3), S. minor (0.73 ± 3.56 ind.m-3), and A. tenuiserrata (0.80 ± 3.63 ind.m-3) were found above the continental shelf, whereas S. danae (0.70 ± 1.67 ind.m-3), S. minor (4.92 ± 17.79 ind.m-3), and A. tenuiserrata (0.90 ± 2.17 ind.m-3) were found above the slope at 1 m depth (Figures 4b, 5a, b, and c). The other species occurred only in deep waters.

Scolecithricella and Scolecithrix were the two most abundant genera and their patterns of vertical distribution reflect the patterns of the Scolecitrichidae family as a whole (Table II). Scolecithricella abundance was highest at 1 and 250 m during the DS, whereas the highest density

of Scolecithrix was mainly in the 1m layer during the RS. Scolecithricella showed an increase in abundance from the surface downward and peaked at 250 m (Table II).

Based on the groups proposed by Kuriyama and Nishida (2006), we classified the scolecitrichid copepods into the following four groups according to the vertical patterns of abundance observed in our study (the seasonal abundance peaks are indicated in parentheses).

group A—epipelagic species (with major abundance in the upper 250 m): Scolecithrix danae (RS), Scolecithricella minor, Amallothrix tenuiserrata, and Lophothrix frontalis (DS).

group B—Upper-mesopelagic species (with major abundance in the upper mesopelagic zone, upper 800 m): Lophothrix quadrispinosa, Scaphocalanus echinatus, Scolecithrix bradyi, Scolecithricella dentata (RS), Racovitzanus levis, Pseudoamallothrix ovata, and Pseudoamallothrix profunda (DS).

group C—Mesopelagic species (species with a broad range in the 800-m layer): Scaphocalanus brevicornis (RS), Lophothrix latipes, and Scottocalanus securifrons (DS).

group D—lower-mesopelagic species (species with a major population below 800 m): Amallothrix dentipes, Scaphocalanus magnus (RS), Scaphocalanus elongatus, and Scaphocalanus subbrevicornis (DS).

The results of the glMs showed that the total scolecitrichid density was related to different environmental parameters. Among the competing models of the glMs, the most plausible model indicated that total scolecitrichid density was positively related to temperature and nitrate, and negatively related to silicate (Table III).

DISCUSSION

HYDROgRAPHICAl INFlUeNCeS ON SCOleCITRICHID ABUNDANCe

evaluation of factors controlling the distribution of zooplankton species is central to determining

Figure 3 - Vertical distribution in the water column of the Campos Basin of the mean values: (a) total density and standard deviation of scolecitrichids (log ind.m-3). Blue bars, rainy season (RS); open bars, dry season (DS), (b) scolecitrichid species richness, diversity, and evenness. Dark blue bars, richness; Navy blue bar, diversity; open bars, evenness. Rainy season (RS) and dry season (DS).



TABLE IIIMultiple regression models of environmental parameters

and the total scolecitrichid density. Tem, temperature; Nit, nitrate; Sil, silicate; AICc, Akaike information criterion;

wi, weight.

Model AICc ΔAICc wi

I (+)Tem/(+)Nit/(-)Sil 38.95 0.00 0.12

II (+)Tem/(-)Sil 39.88 0.92 0.07

Figure 4 - Study area, showing the seasonal variation of Scolecithrix danae (ind.m-3) at 1 m depth, during the rainy season (a) and dry season (b).

the biological and ecological functioning of aquatic ecosystems. Although it is generally difficult to identify the main factors that explain variation in zooplankton abundance (Pinel-Alloul 1995), abiotic factors such as salinity, temperature, nutrients, DO, and pH have been identified as critical in the development of zooplankton (Quetin et al. 1996). In the present study, the distribution and abundance of scolecitrichids were related to the different oceanographic conditions that occur in the studied area. The abundance of scolecitrichids observed at a depth of 1 m over the continental shelf was positively related to changes in temperature and nitrate, and negatively influenced by the nutrient silicate. Within our study region, the upper water

mass (TW) has the highest temperatures and the lowest nutrient values (Zalmon et al. 2015, Suzuki et al. 2015), which supports the hypothesis of the influence of different water masses on this copepod assemblage. The low supply of available nutrients is very transitory and small portions are derived from the decomposition of organic matter in the photic zone (Metzler et al. 1997).

The spatial distribution of oceanic organisms is determined by the interactions between organism behavior and physical oceanographic structure and processes (McManus and Woodson 2012). According to Siokou-Frangou et al. (1997), temperature fluctuations regulate the life history of all copepod species. Temperature modifies the reproductive capabilities of crustaceans in many ways (Smyly 1974). Within a suitable range, increases in temperature will increase egg production and growth rate, and shorten reproductive cycle and hatching time. However, different species living in different geographical regions may have specific temperature requirements (li et al. 2009). According to Halsband-lenk et



al. (2002), the thermal tolerances of survival, reproduction and development may at least partly determine horizontal and seasonal distribution patterns of different species. Consistent with our findings for scolecitrichids in the northern region of Rio de Janeiro, the population size of several other copepods, e.g., Oithona, Paracalanus, and Acartia in Japan, and Labidocera in China, has been reported to increase with increasing temperature (Chang and Fang 2004). According to these authors, environmental factors are known to affect the distribution, species composition, and abundance of copepods.

ABUNDANCe, OCCURReNCe, AND VeRTICAl DISTRIBUTION OF SCOleCITRICHIDAe COPePODS

A vertical distribution pattern is commonly observed in oceanic mesozooplankton, characterized by an overall decline in numbers and biomass with increasing depth in the deep sea (Weikert et al. 2001, and references therein). The results obtained in the present study are consistent with the pattern reported in vertical distribution studies in oceanic areas of the Southwestern Atlantic Ocean (Dias et al. 2010, 2018, Bonecker et al. 2014, 2018), with a decrease in density and an increase in diversity and richness with depth. The same pattern was observed by Weikert et al. (2001) and Siokou-Frangou et al. (2013) for deep-sea plankton communities in the oligotrophic levantine Sea in the eastern Mediterranean.

Dominance is often considered indicative of successful evolution (Madhupratap and Haridas 1986, Briggs 1974). Despite their known vertical distribution pattern (Table IV), in this study the major populations of S. danae, S. minor, A. tenuiserrata, and L. frontalis were recorded in the upper 250 m, in neritic as well as oceanic waters.

Copepods consume marine snow or particles attached to it. Appendicularians are also important contributors to the vertical flux through fecal

Figure 5 - Study area, showing the seasonal variation of scolecitrichid species (ind.m-3) at 1 m depth, during the dry season. Lophothrix frontalis (a), Scolecithricella minor (b), and Amallothrix tenuiserrata (c).



pellets and houses (Turner 2015). Scolecitrichids such as S. minor, one of the most frequent and abundant scolecitrichids in the region, are typically considered to be detritus feeders (Yamaguchi et al. 1999). While no quantitative data on detrital abundance in the Campos Basin are available at present, the concentration of suspended particulate matter was lower in deep water than in shallow water (Pedrosa et al. 2006). In our study region, appendicularians (mostly Oikopleura longicauda) are an abundant mesozooplanktonic group, with higher densities in the upper layers (Bonecker et al. 2014, 2018, Carvalho and Bonecker 2016). A high abundance of appendicularians at 1 m depth implies a high production rate of discarded “houses” (a source of detritus) that can be an important dietary component for Scolecitrichidae copepods (Ferrari and Steinberg 1993, Yamaguchi et al. 1999).

All the dominant Scolecitrichidae species showed the vertical patterns of abundance of epipelagic species and can be considered epipelagic migrants due to their distribution throughout the entire water column (1, 250, 800, and 1,200 m). The other species were considered mesopelagic zone dwellers.

Scolecithrix danae is numerically the most abundant and widespread species of Scolecitrichidae and is relatively common in the surface and subsurface layers during both the day and night (T.C. gopalakrishna, unpublished data). In the present study, S. danae was found throughout the water column down to a depth of 1,200 m, with higher abundances being recorded in the 1m layer in both sampling periods. Vervoort (1965) detected S. danae inhabiting intermediate and subsurface layers, closer to the surface at night and in comparatively deep water during the day. This species was also recorded by Wheeler (1970) at depths between 4,100 and 2,200 m.

Scolecithricella minor is a small calanoid copepod widely distributed throughout the high latitude seas of both the northern and southern

hemispheres, occurring in the epi- and mesopelagic zones (Roe 1984). However, despite the widespread distribution and potential importance of S. minor in the trophodynamics of pelagic systems, information on its life cycle is extremely limited (Yamaguchi et al. 1999). Scolecithricella minor is typically considered a detritus feeder, and in the southern Japan Sea is distributed below the thermocline in the daytime and ascends at night (Yamaguchi et al. 1999). These authors recorded the distribution of this species to depths of 700 m, with an abundance peak between 100 and 400 m. In our study, this species was found during both sampling periods, with greater abundance being recorded in the 1 m and 250 m layers, mainly during the DS.

Amallothrix tenuiserrata was recorded only during the DS. It was found in greater abundance in the 1m and 250m depth levels, with reduced densities in the 1,200m layer. In a study of zooplankton in which day–night samples were collected from the euphotic zone of the Indian Ocean, gopalakrishnan (T.C. gopalakrishna, unpublished data) considered this species to be a strong migrant, undertaking nocturnal migrations in neritic and oceanic waters. Amallothrix tenuiserrata inhabits intermediate depths up to the surface, and according to gopalakrishnan (T.C. gopalakrishna, unpublished data), in the Indian Ocean this species is most abundant in the highly saline upwelling waters of the Arabian Sea and warm tropical low saline surface waters of the Bay of Bengal. The occurrence of A. tenuiserrata only during the DS in the present study can be related to unstable conditions due to the mobility of the TW-SACW interface, an increase in which is associated with the higher temperatures of the ocean–atmosphere interface (Tsuchiya et al. 1994, Mémery et al. 2000).

Although Lophothrix frontalis may be classified as epipelagic–abyssopelagic, in the present study this species was found mainly in the subsurface water during the DS. gopalakrishnan (T.C. gopalakrishna,



unpublished data) found that, in the north Indian Ocean, L. frontalis inhabits high-salinity intermediate and deep waters, rising to the surface layers during the night. This author found L. frontalis only in night hauls, and the total absence in day hauls indicated its nocturnal occurrence in surface waters, consistent with diurnal vertical migration. In our study, all samples were collected during the night and this can explain the higher abundance of L. frontalis in 1-m-depth samples compared to the deeper samples. Remarkably, even some meso- and bathypelagic scolecitrichid species ascend to the surface as a part of the diurnal migration (gopalakrishnan and Balachandran 1992, Kuriyama and Nishida 2006, and references therein).

Of the species classified as mesopelagic, Amalothrix dentipes, Lophothrix quadrispinosa, and Racovitzanus levis have only recently been recorded from the Southwestern Atlantic Ocean (Bonecker et al. 2014). In the present study, the upper-mesopelagic species L. quadrispinosa has been reported at 250 m depths over the SACW influence, during the RS, and at 1,200 m over the UCDW influence during the DS. This species has also been reported from the North Atlantic, South Pacific, and Indian oceans (Bradford-Grieve et al. 1999, Razouls et al. 2005-2018), and Owre and Foyo (1964) reported its occurrence at depths of 584 m and 1,750 m in the Florida region. Racovitzanus levis, which in the present study was collected at 250 m depths over the SACW influence during the

TABLE IVScolecitrichid copepod distribution range (m) in the study area, classification according to the references (E, epipelagic; M, mesopelagic; B, bathypelagic; A, abyssopelagic), and references relating to the occurrence of scolecitrichid copepods:

Southwestern Atlantic (1, Björnberg 1963; 2, Björnberg 1965; 3, Campaner 1984; 4, Campaner 1985), other localities (1, Grice and Hulsemann 1965; 2, Roe 1972; 3, Gopalakrishnan (T.C. Gopalakrishna, unpublished data); 4, Roe 1984; 5, Madhupratap and Haridas 1986; 6, Bradford-Grieve et al. 1999; 7, Yamaguchi et al. 1999; 8, Kuriyama and Nishida

2006; 9, Razouls et al. 2005-2018).

Species Distribution range Classification Southwestern Atlantic Other localities

Amallothrix dentipes 800 and 1,200 M-B 4/6/9Amallothrix tenuiserrata 1, 250 and 1,200 e 3/4 3/5/6/9

Lophothrix frontalis 1, 250, 800 and1,200 e-A 2 2/3/6/8/9Lophothrix latipes 800 e-B 4 4/6/9

Lophothrix quadrispinosa 250, 800 and 1,200 M-B 6/9Pseudoamallothrix ovata 250 e-M 3/4 3/4/6

Pseudoamallothrix profunda 250 M-B 3/4 2/6/8/9Racovitzanus levis 250 M 1/2/9

Scaphocalanus brevicornis 800 e-B 2 1/2/4/6/8/9Scaphocalanus echinatus 250 and 800 e-B 3/4 1/2/3/6/8/9Scaphocalanus elongatus 1,200 M-A 1/2/6/8/9Scaphocalanus magnus 800 and 1,200 e-B 1/2/4/6/8/9

Scaphocalanus subbrevicornis 1,200 M-B 2 2/6/8/9Scolecithrix danae 1, 250, 800 and 1,200 e-M 1/2/4 1/2/3/5/6/8/9Scolecithrix bradyi 250 and 1,200 e-M 2/4 1/2/3/5/6/8/9

Scolecithricella dentata 250, 800 and 1,200 e-M 1/2/3/4 1/2/3/4/5/6/8/9Scolecithricella minor 1, 250, 800 and 1,200 e-B 4/6/7/9

Scottocalanus securifrons 250 and 800 e-B 4 2/3/4/5/6/8/9



DS, has also been reported from the North Atlantic, Pacific, and Indian oceans (Harding 1974, Razouls et al. 2005-2018). Roe (1972) reported this species off the Canary Islands (North Atlantic) at depths of 450 m in diurnal hauls and 360 m in night hauls, whereas in the northeast Atlantic, grice and Hulsemann (1965) found specimens of R. levis at depths of 400–1,000 m, and Deevey and Brooks (1977) recorded its presence at depths between 0 and 1000 m in the Sargasso Sea off Bermuda. Furthermore, Harding (1974) cited the occurrence of R. levis in a vertical tow at 3,000–4,000 m.

In our study, the lower-mesopelagic species A. dentipes was collected at 1,200 m, above the UCDW influence, during the RS, and at 800 and 1,200 m depths during the DS. This species has also been reported from the Central South Atlantic, South Pacific, and Indian oceans, and the Antarctic and Sub-Antarctic regions (Bradford 1973, Bradford-grieve et al. 1999, Razouls et al. 2000). According to Bradford-grieve et al. (1999), this species typically occurs in Antarctic waters, occasionally reaching the Convergence, and more rarely in the Southern Atlantic (36°). In the North east Atlantic, Roe (1984) reported the occurrence of A. dentipes at 250–600 m depths.

Divergences between the occurrences of species recorded in the present study (water masses below 250 m depth) and those reported previously could be attributed to the circulation of water masses, which may have been a potential vehicle of dispersal for these species. Amalothrix dentipes and L. quadrispinosa are classified as meso-bathypelagic, and R. levis as mesopelagic. As few species have restricted areas of abundance, inconsistencies in the distributions of these species indicate that the data available are still too limited to demarcate the zones of occurrence of most species, in view of the lack of studies in deep habitats in the Southwestern Atlantic Ocean.

Data on Scolecitrichidae species are limited and scattered, with only a few previous studies

available for comparison with the present results on the vertical distribution of each species (Table IV). Kuriyama and Nishida (2006) studied the distribution patterns of 43 scolecitrichid species occurring in Sagami Bay from the surface down to 1,000 m depth. Although the vertical ranges of hauls were smaller, the depth distributions in Sagami Bay are similar to those observed in the present study for most of the 11 common species compared. Both Kuriyama and Nishida (2006) and the present study recorded S. brevicornis, S. echinatus, S. danae, S. bradyi, S. dentata, and S. securifrons in deeper strata. Yamaguchi et al. (1999) analyzed the vertical migration, population structure, and life cycle of Scolecithricella minor in Toyama Bay (southern Sea of Japan) and found a vertical distribution pattern comparable to the distribution recorded in the present study. Roe (1984) reported the vertical distribution patterns of 14 species, sampled through hauls performed at four depths (100, 250, 450, and 600 m) in the Northeast Atlantic. Seven of the species recorded in this study showed vertical distribution patterns that were narrower than those recorded in the present study. The same author (Roe 1972), has reported vertical patterns, with respect to the day–night distribution, off the Canary Islands that are comparable to the distribution patterns of 13 species recorded in the present study. Racovitzanus levis, Scaphocalanus brevicornis, and Scaphocalanus elongatus, which were distributed in the mesopelagic layers in the present study, have been found to occur only in much deeper layers (below 5,000 m) in the northeast Atlantic (grice and Hulsemann 1965).

CONCLUSIONS

The aim of this paper was to review our current understanding of scolecitrichid copepod biodiversity in the northern region of Rio de Janeiro State. In the present study, we recognized the following patterns in the species diversity of scolecitrichids



in relation to their depth distribution, abundance, and taxonomic groupings: (1) contrasting vertical patterns between abundance and species diversity, which is a common phenomenon in pelagic copepods in general, being repeated in all genera and in the family as a whole; and (2) a trend of vertical segregation in a small number of epipelagic migrants in contrast to a considerably larger number of meso- and bathypelagic nondominant species. These patterns suggest that the scolecitrichid assemblages in the region may be structured, and that this is mainly due to the partitioning of vertical habitats and food resources.

ACKNOWLEDGMENTS

This study is part of the Habitats Project - Campos Basin environmental Heterogeneity by CeNPeS/PeTROBRAS. The authors thank the team of the Zooplankton and Ichthyoplankton Integrated laboratory of Universidade Federal do Rio de Janeiro, in particular Cláudio de S. Ressur and José R.S. Silva for sorting the samples. We also wish to thank Dr. luiz Fernando loureiro Fernandes and Suzanna Vianna for help with identification, and the Drs. Rodolfo Paranhos and Marina Satika Suzuki for providing environmental parameters. Finally, we wish to thank PeTROBRAS, which made possible the sampling and material analyses.

AUTHOR CONTRIBUTIONS

SLCB designed the study, participated in fieldwork and revised the paper; COD and AVA analyzed the data and wrote the paper.

REFERENCES

BeRASATegUI AD, MeNU MARQUe S, gÓMeZ-eRACH M, RAMÍReZ FC, MIANZAN HW AND ACHA eM. 2006. Copepod assemblages in a highly complex hydrographic region. estuar Coast Shelf Sci 66: 483-492.

BJÖRNBeRg TSK. 1963. On the marine free-living copepods off Brazil. Bolm Inst Oceanogr S Paulo 13: 3-142.

BJÖRNBeRg TSK. 1965. The study of planktonic copepods in the South West Atlantic. An Acad Bras Cienc 37: 219-230.

BONeCKeR ACT, DIAS CO, De CASTRO MS, De CARVAlHO PF, ARAUJO AV, PARANHOS R, CABRAl AS AND BONeCKeR SlC. 2018. Vertical distribution of mesozooplankton and ichthyoplankton communities in the South-western Atlantic Ocean (23°14′1″S 40°42′19″W). J Mar Biol Assoc UK, p. 1-15.

BONeCKeR SlC, ARAUJO AV, CARVAlHO PF, DIAS CO, FeRNANDeS lFl, MIgOTTO Ae AND De OlIVeIRA OMP. 2014. Horizontal and vertical distribution of mesozooplankton species richness and composition down to 2,300 m in the southwest Atlantic Ocean. Zoologia 31: 445-462.

BOXSHAll gA AND HAlSeY SH. 2004. An introduction to copepod diversity. london: The Ray Society, 966 p.

BRADFORD J. 1973. Revision of family and some generic definitions in the Phaennidae and Scolecithricidae Copepoda: Calanoida. New Zeal J Mar Fresh 7(1-2): 133-152.

BRADFORD-gRIeVe JM, MARKHASeVA eI, ROCHA CeF AND ABIAHY B. 1999. Copepoda. In: Boltovskoy D (ed), South Atlantic zooplankton. leiden: Backhuys Publishers, p. 869-1098.

BRIggS JC. 1974. Marine Zoogeography. New York: Mcgraw-Hill, 475 p.

BURNHAM KP AND ANDeRSON DR. 2002. Model Selection and Multimodel Inference. A Practical Information-Theoretic Approach. New York: Springer-Verlag, 488 p.

CAMPANeR AF. 1984. Scaphocalanus and Scolecithricella.Copepoda, Calanoida, Scolecithricida. from the epipelagial off southern Brazil: a taxonomic and distributional survey. Bolm Zool 8: 165-187.

CAMPANeR AF. 1985. Occurrence and distribution of copepods. Crustacea in the epipelagial off Southern Brazil. Bolm Inst Oceanogr S Paulo 33: 5-27.

CARVAlHO PF AND BONeCKeR SlC. 2016. Variação da composição e abundância das espécies da Classe Appendicularia e seu uso como potenciais bioindicadoras de regiões e massas de água superficiais na área da Bacia de Campos, Rio de Janeiro, Brasil. Iheringia Sér Zool 106: e2016022.

CHANg W AND FANg l. 2004. Temporal and spatial variations in the species composition, distribution and abundance of copepods in Kaohsiung Harbor, Taiwan. Zool Stu 43: 454-463.

ClARKe KR AND gORleY RN. 2006. PRIMeR v6: User Manual/Tutorial. Plymouth: PRIMeR-e, 190 p.

DeeVeY gB AND BROOKS Al. 1977. Copepods of the Sargasso Sea off Bermuda: species composition, and vertical and seasonal distribution between the surface and 2000 m. Bull Mar Sci 27: 256-291.



DIAS CO AND ARAUJO AV. 2006. Copepoda. In: Bonecker SlC (ed), Atlas do zooplâncton da região central da Zona econômica exclusiva. Série livros/Documentos ReVIZee Score Central. Rio de Janeiro: Museu Nacional 21: 21-99.

DIAS CO, ARAUJO AV AND BONeCKeR SlC. 2018. Vertical distribution and structure of copepod (Arthropoda: Copepoda) assemblages in two different seasons down to 1,200 m in the tropical Southwestern Atlantic. Zoologia 35: e13886.

DIAS CO, ARAUJO AV, PARANHOS R AND BONeCKeR SlC. 2010. Vertical copepod assemblages (0–2300 m) off southern Brazil. Zool Stud 49: 230-242.

DIAS CO, ARAUJO AV, VIANNA SC, FeRNANDeS lFl, PARANHOS R, SUZUKI MS AND BONeCKeR SlC. 2015. Spatial and temporal changes in biomass, production and assemblage structure of mesozooplanktonic copepods in the tropical south-west Atlantic Ocean. J Mar Biol Assoc UK 95: 483-496.

el-SHeRBINY MM AND Al-AIDAROOS AM. 2013. First record and redescription of Macandrewella cochinensis gopalakrishnan, 1973. Copepoda, Scolecitrichidae. from the Red Sea, with notes on swarm formation. ZooKeys 344: 1-15.

eSKINAZI-SANT’ANNA eM AND BJÖRNBeRg TKS. 2006. Seasonal dynamics of microzooplankton in the São Sebastião Channel. Brazil Braz J Biol 66: 221-231.

FeRRARI FD AND MARKHASeVA el. 2000. A new genus and species of Scolecitrichid Calanoid Copepod. Crustacea from a hydrothermal vent along the Southern east Pacific rise. Proc Biol Soc Wash 113: 1079-1088.

FeRRARI FD AND STeINBeRg DK. 1993. Scopalatum vorax (esterly, 1911) and Scolecithricella lobophora Park, 1970, calanoid copepods (Scolecitrichidae) associated with a pelagic tunicate in Monterey Bay. Proc Biol Soc Wash 106: 467-489.

gOPAlAKRISHNAN TC AND BAlACHANDRAN T. 1992. North-south diversity of Scolecithricidae species. Copepoda: Calanoida in the Indian Ocean. In: Desai BN (ed), Oceanography of the Indian Ocean, p. 167-175.

gOPAlAKRISHNAN TC AND DeVI KS. 1998. Distribution of Scolecithricidae (Copepoda: Calanoida) in the Indian Ocean. In: Pierrot-Bults AC and Spoel SV (eds), Pelagic Biogeography ICoPB II. Proceedings of the 2nd International Conference. Final report of SCOR/IOC working group 93. Workshop Report N° 142. UNeSCO, Noordwijkerhout, The Netherlands, p. 127-136.

gRASSHOFF K, eHRHARDT M AND KReMlINg K. 1999. Methods of seawater analysis. 2nd ed., Weinheim/Deeerfield Beach, Florida: Verlag Chemie, 419 p.

gRICe gD AND HUlSeMANN K. 1965. Abundance, vertical distribution and taxonomy of calanoid copepods

at selected stations in the northeast Atlantic. J Zool 146: 21-262.

HAlSBAND-leNK C, HIRCHe HJ AND CARlOTTI F. 2002. Temperature impact on reproduction and development of congener copepod populations. J exp Mar Biol ecol 271: 121-153.

HARDINg gCH. 1974. The food of deep-sea copepods. J Mar Biol Assoc UK 54: 141-156.

KURIYAMA M AND NISHIDA S. 2006. Species diversity and niche-partitioning in the pelagic copepods of the family Scolecitrichidae. Calanoida. Crustaceana 79: 293-317.

lI Cl, lUO XX, HUANg XH AND gU BH. 2009. Influences of temperature on development and survival, reproduction and growth of a calanoid copepod (Pseudodiaptomus dubia). Sci World J 9: 866-879.

lOPeS RM, KATSURAgAWA M, MONTÚ MA, MUelBeRT JH, DIAS JF, gORRI C AND BRANDINI FP. 2006. Zooplankton and ichthyoplankton distribution on the southern Brazilian shelf: an overview. Sci Mar 70: 189-202.

MADHUPRATAP M AND HARIDAS P. 1986. epipelagic calanoid copepods of the northern Indian Ocean. Oceanol Acta 9: 105-117.

MARKHASeVA el AND DAHMS HU. 2004. P l e s i o s c o l e c i t h r i x ( C o p e p o d a , C a l a n o i d a , Scolecitrichidae): a new genus, and a new species from the high Antarctic Weddell Sea. Southern Ocean. Sarsia 89: 32-337.

MCeWeN gF, JOHNSON MW AND FOlSOM TR. 1957. A statistical analysis of the performance of the Folsom plankton sample splitter, based upon test observations. Arch Meteor geophys Biochem Bioklimatol 7: 502-527.

MCMANUS MA AND WOODSON CB. 2012. Plankton distribution and ocean dispersal. J exp Biol 215: 1008-1016.

MÉMeRY lM, ARHAN XA, AlVAReZ-SAlgADO MJ, MeSSIA H, MeRCIeR Cg, CASTRO A AND RIOS F. 2000. The water masses along the western boundary of the south and equatorial Atlantic. Prog Oceanogr 47: 69-98.

MeTZleR PM, gIlBeRT PM, gAeTA AS AND lUBlAN J. 1997. New and regenerated production in the South Atlantic off Brazil. Deep-Sea Res 44: 363-384.

NISHIDA S AND OHTSUKA S. 1997. Ultrastructure of the mouthpart sensory setae in mesopelagic copepods of the family Scolecitrichidae. Plankton Biol ecol 44: 81-90.

OHTSUKA S, NISHIDA S AND NAKAgUCHI K. 2002. Three new species of the genus Macandrewella (Copepoda: Calanoida: Scolecitrichidae) from the Pacific Ocean, with notes on distribution and feeding habits. J Nat Hist 36: 531-564.

OWRe HB AND FOYO M. 1964. Plankton of the Florida Current. Part IX. Additions to the list of Copepoda, with descriptions of two rare species. Bull Mar Sci gulf Caribb 14: 342-358.



PeDROSA P, PARANHOS R, SUZUKI MS, ANDRADe l, SIlVeIRA ICA, SCHMIDT ACK, FAlCÃO APC, lAVRADO HP AND ReZeNDe Ce. 2006. Hidroquímica de massas de água oceânicas em regiões da margem continental brasileira Bacia de Campos (estado do Rio de Janeiro, Brasil). geochim Brasil 20: 104-122.

PINel-AllOUl B. 1995. Spatial heterogeneity as a multiscale characteristic of zooplankton community. Hydrobiologia 300/301: 17-42.

QUeTIN lB, ROSS RM, FRAZeR TK AND HABeRMAN Kl. 1996. Factors affecting distribution and abundance of zooplankton, with an emphasis on antarctic krill, Euphausia superba. Antarct Res Ser 70: 357-371.

R CORe TeAM. 2015. R Core Team. R: a language and environment for Statistical Computing (Version 3.1.3). Vienna: R Foundation for Statistical Computing.

RAZOUlS C, De BOVÉe F, KOUWeNBeRg J AND DeSReUMAUX N. 2005-2018. Diversity and geographic distribution of marine planktonic copepods. Available at: http://copepodes.obs-banyuls.fr/en. Accessed on December 3, 2018.

RAZOUlS S, RAZOUlS C AND De BOVÉe F. 2000. Biodiversity and biogeography of Antarctic copepods. Antarctic Sci 12: 343-362.

RODRIgUeS SV, MARINHO MM, JONCK CCC, gONÇAlVeS eS, BRANT VF, PARANHOS R, CURBelO MP AND FAlCÃO AP. 2014. Phytoplankton community structures in shelf and oceanic waters off southeast Brazil (20º–25ºS), as determined by pigment signatures. Deep-Sea Res I 88: 47-62.

ROe HSJ. 1972. The vertical distributions and diurnal migrations of calanoid copepods collected on the SOND Cruise, 1965. I. The total population and general discussion. J Mar Biol Assoc UK 52: 277-314.

ROe HSJ. 1984. The diel migrations and distributions within a mesopelagic community in the North east Atlantic. 4. The copepods. Progr Oceanogr 13: 353-388.

SIlVeIRA ICA, SCHMIDT ACK, CAMPOS eJS, gODOI SS AND IKeDA YA. 2000. Corrente do Brasil ao largo da costa leste Brasileira. Braz J Oceanogr 48: 171-183.

SIOKOU-FRANgOU I, CHRISTOU eD, FRAgOPOUl N AND MAZZOCCHI Mg. 1997. Mesozooplankton distribution from Sicily to Cyprus (easter Mediterranean): II Copepod assemblages. Oceanol Acta 20: 537-548.

SIOKOU-FRANgOU I, ZeRVOUDAKI S AND CHRISTOU eD. 2013. Mesozooplankton community distribution down to 1000 m along a gradient of oligotrophy in the eastern Mediterranean Sea (Aegean Sea). J Plankton Res 35: 1313-1330.

SMYlY WJP. 1974. The effect of temperature on the development time of the eggs of three freshwater cyclopoid copepods from the english lake District. Crustaceana 27: 278-284.

STeINBeRg DK. 1995. Diet of copepods. Scopalatum vorax. associated with mesopelagic detritus. giant larvacean houses in Monterey Bay, California. Mar Biol 122: 571-584.

STRAMMA l, IKeDA Y AND PeTeRSON Rg. 1990. geostrophic transport in the Brazil Current region north of 20°S. Deep-Sea Research 37: 1875-1886.

SUZUKI MS, ReZeNDe Ce, PARANHOS R AND FAlCÃO AP. 2015. Spatial distribution vertical and horizontal and partitioning of dissolved and particulate nutrients (C, N and P) in the Campos Basin, Southern Brazil. est Coastal Shelf Sci 166: 4-12.

TSUCHIYA M, TAlleY lD AND MCCARTNeY MS. 1994. Water-mass distributions in the western South Atlantic; A section from South georgia Island (54°S) northward across the equator. J Mar Res 52: 55-81.

TURNeR JT. 2015. Zooplankton fecal pellets, marine snow, phytodetritus and the ocean’s biological pump. Prog Oceanogr 130: 205-248.

VeRVOORT W. 1965. Pelagic Copepoda. Part II. Copepoda Calanoida of the families Phaennidae up to and including Acartiidae. Atlantide Rep 8: 9-216.

VIANA AR, FAUgeÈReS JC, KOWSMANN RO, lIMA JAM, CADDAAH lFg AND RIZZO Jg. 1998. Hydrology, morphology and sedimentology of the Campos continental margin, offshore Brazil. Sediment geol 115: 133-157.

VYSHKVARTZeVA NV. 2001. A key to the genera of Scolecitrichidae, with description of a new genus and redescription of two species. Crustacea, Calanoida. Zoosyst Rossica 9: 77-98.

WeIKeRT H, KOPPelMANN R AND WIegRATZ S. 2001. evidence of episodic changes in deep-sea mesozooplankton abundance and composition in the levantine Sea eastern Mediterranean. J Marine Syst 30: 221-239.

WHeeleR JR eH. 1970. Atlantic deep-sea calanoid Copepoda. Smithson. Contr Zool 55: 1-31.

WISHNeR KF, gelFMAN C, gOWINg MM, OUTRAM DM, RAPIeN M AND WIllIAMS Rl. 2008. Vertical zonation and distributions of calanoid copepods through the lower oxycline of the Arabian Sea oxygen minimum zone. Prog Oceanogr 78: 163-191.

YAMAgUCHI A, IKeDA T AND HIRAKAWA K. 1999. Diel vertical migration, population structure and life cycle of the copepod Scolecithricella minor (Calanoida: Scolecitrichidae) in Toyama Bay, southern Japan Sea. Plankton Biol ecol 46: 5-61.

ZAlMON IR, De ReZeNDe Ce, VelOSO Vg, SAllOReNZO I, PARANHOS R, FAlCÃO AP AND De AlMeIDA TCM. 2015. Influence of estuarine dynamics on macrobenthos spatial variability along the southeast continental shelf of Brazil. Sci Mar 79: 379-391.

Distribution, diversity, and habitat partitioning of ...

Documents

Transcript of Distribution, diversity, and habitat partitioning of ...